Ximen Mining Corp. (TSX-V:XIM
) (the "Company" or
"Ximen") is pleased to announce the final results from the fall
2014 diamond drill program on the Brett epithermal gold property in
southern B.C. In total, 2977 m of drilling was completed in 13
holes. All of the holes were drilled to test new targets that were
untested, or only minimally tested, by historic work on the
property.
Highlights include:
- Two new high-grade gold-bearing veins discovered.
Results include 34.18 g/t Au over 0.9 m from one
zone and 16.7 g/t Au over 1.5 m from the second.
- Significant intervals of bulk tonnage gold
mineralization intercepted, including 1.77 g/t Au
over 31 m, 1.88 g/t Au over 16.55 m and 0.82 g/t Au over 33
m.
- Two drill holes ended in intervals of low grade gold
mineralization which remain open to
depth.
- Widespread alteration, with strong epithermal
pathfinder geochemistry, identified in several
areas.
- Trace element geochemistry provides vectors for
follow-up drilling.
- High grade gold values confirmed from the Main Zone,
including 24.7 g/t Au over 1.3 m
Results for weighted average gold values are reported below. A
discussion of these results follows.
Hole |
|
From |
To |
Interval |
Au |
Ag |
|
|
|
metres |
metres |
metres |
g/t |
g/t |
|
B14-01 |
|
43.00 |
50.20 |
7.20 |
2.85 |
7.73 |
|
B14-01 |
including |
47.00 |
49.20 |
2.20 |
7.31 |
20.09 |
MAIN ZONE |
B14-01 |
|
124.00 |
135.80 |
11.80 |
0.57 |
2.27 |
|
B14-01 |
|
146.95 |
147.85 |
0.90 |
34.18 |
6.66 |
490 GOLD ZONE |
|
|
|
|
|
|
|
|
B14-02 |
|
112.20 |
118.30 |
6.10 |
0.25 |
0.85 |
|
B14-02 |
|
162.60 |
167.30 |
4.70 |
0.54 |
0.65 |
490 GOLD ZONE |
B14-02 |
|
202.00 |
222.50 |
22.00 |
0.43 |
1.33 |
End of hole; zone open to depth |
|
|
|
|
|
|
|
|
B14-03 |
|
113.60 |
117.60 |
4.00 |
0.32 |
1.01 |
|
|
|
|
|
|
|
|
|
B14-04 |
|
21.70 |
33.80 |
12.10 |
0.46 |
2.24 |
|
B14-04 |
|
47.30 |
78.30 |
31.00 |
1.77 |
2.13 |
|
B14-04 |
including |
54.90 |
56.20 |
1.30 |
24.70 |
6.57 |
MAIN ZONE |
B14-04 |
|
128.90 |
133.60 |
4.70 |
1.40 |
2.72 |
|
|
|
|
|
|
|
|
|
B14-05 |
|
51.00 |
84.00 |
33.00 |
0.82 |
1.27 |
|
B14-05 |
including |
55.80 |
56.30 |
0.50 |
12.10 |
6.00 |
MAIN ZONE |
B14-05 |
|
141.45 |
158.00 |
16.55 |
1.88 |
2.79 |
|
B14-05 |
including |
155.00 |
156.00 |
1.00 |
20.50 |
5.06 |
490 GOLD ZONE |
|
|
|
|
|
|
|
|
B14-06 |
|
22.20 |
27.20 |
5.00 |
0.60 |
0.85 |
|
B14-06 |
|
79.00 |
85.00 |
6.00 |
0.30 |
0.94 |
|
|
|
|
|
|
|
|
|
B14-07 |
|
322.00 |
324.00 |
4.00 |
0.49 |
1.28 |
End of hole; zone open to depth |
|
|
|
|
|
|
|
|
B14-11 |
|
189.65 |
190.15 |
0.50 |
1.03 |
34.20 |
GOSSAN ZONE |
|
|
|
|
|
|
|
|
B14-13 |
|
49.00 |
55.00 |
6.00 |
0.42 |
1.89 |
|
B14-13 |
|
174.50 |
179.50 |
5.00 |
5.31 |
2.50 |
|
B14-13 |
including |
176.00 |
177.50 |
1.50 |
16.70 |
6.56 |
NEW DISCOVERY |
Gold mineralization on the property is hosted within flat-lying
to gently-dipping interlayered Eocene volcanics and volcaniclastics
and is controlled both by structure and stratigraphy. Vein and
stockwork mineralization occurs preferentially in competent
lithologies that are cut by steep, generally west dipping,
structures. Within these competent lithologies, alteration
envelopes to zones of veining are generally narrow. Bulk tonnage
gold mineralization develops where these gold-bearing feeder
structures pass through more permeable volcaniclastic or volcanic
units. Gold-bearing fluids travel laterally from the feeder
structure into these permeable horizons, particularly when those
horizons are constrained by an overlying impermeable volcanic cap.
The mineralization is controlled by proximity to the feeder
structure, by permeability of the host unit, and by the nature of
the cap rock.
Multi-element data from drilling indicates that zones of gold
mineralization have a distinctive trace element signature comprised
of Au:Ag:As:Mo. At higher levels and distally from gold zones,
alteration has a markedly different geochemical signature,
comprised of Hg:Mo:As:Sb:Tl. This trace element geochemistry
provides a useful vector for follow-up drilling.
To view an enhanced version of Figure 1: Brett
Gold Property in Southern British Columbia, please visit:
http://orders.newsfilecorp.com/files/3028/14278_ximen.2.jpg
Holes B14-01 through B14-05 were drilled to test a new vein
target, the 490 Gold Zone. The 490 Gold Zone is located east of the
Main Zone (the subject of most of the historic drilling on the
property) and is a sub-parallel structure located 85 m into the
footwall of the Main Zone. The 490 Gold Zone can be traced on
surface for several hundred metres and was tested by drilling for
only a 100 m strike length near the southern portion of its known
strike extent. Holes were eastward-directed, drilling through the
Main Zone, then continuing in the footwall of the Main Zone, to
test the 490 Gold Zone to the east. In addition to intersecting
discrete epithermal veins, several of the drill holes intersected
broader intervals of strong silica-flooding and low-grade gold
mineralization within more permeable tuffaceous units and breccia
zones. High grade gold values from structurally controlled targets
include 0.90 m grading 34.18 g/t Au and 1.0 m grading 20.5 g/t Au
from the 490 Gold Zone, and 1.3 m grading 24.7 g/t Au from the Main
Zone. Bulk tonnage targets included 16.55 m grading 1.88 g/t Au,
including and adjacent to the 490 Gold Zone and 31 m grading 1.77
g/t Au, including and adjacent to the Main Zone. Also of interest
is a 22.0 m interval at the end of hole B14-02 which graded 0.43
g/t Au and remains open to depth. This horizon should be traced
laterally towards the controlling 490 feeder structure, to explore
for an increase in gold grade more proximal to the structure, and
to establish the full thickness of the permeable horizon.
Hole B14-06 was drilled to test the Border Zone, another new
discovery on the property. It is the first and only hole to test
this target. Multiple zones of silicification, clay alteration,
brecciation and pyrite mineralization, measuring up to 28 m in core
length, were intersected, before the hole bottomed in a thick
Eocene intrusive. Alteration occurs preferentially in permeable
volcaniclastic units within the stratigraphic package. Gold was
elevated throughout the upper 190 m portion of this drill hole,
with several intervals exceeding the cut-off limit chosen for
reporting in the above table, including 5 m grading 0.6 g/t Au and
6 m grading 0.3 g/t Au. Further drilling is warranted to trace
permeable horizons towards feeder structures, where gold may be
better concentrated.
Hole B14-13 was collared approximately 250 m west of the Main
Zone and 250 m south of hole B14-06, to test the area south of the
Border Zone and to intersect the Main and 490 Zones approximately
150 m down-dip from hole B14-05. A new zone of gold mineralization
was discovered in hole B14-13 which graded 5.31 g/t Au over 5 m,
including 1.5 m grading 16.7 g/t Au. This new zone is located
approximately 50 m in the hanging wall of the Main Zone and is
untested by any other drill hole. It is a high priority for further
drilling both as a high-grade vein-style target, and as a possible
feeder structure to bulk tonnage targets in the more permeable
altered volcaniclastic units encountered within this hole and
within hole B14-06.
Holes B14-08 through B14-11 were drilled 1 km to the northeast
of the Main Zone. Drilling targeted a geophysical anomaly (magnetic
low, chargeability high) near the Gossan Zone. Intensely silicified
and pyritic rock is exposed on surface at the Gossan Zone, along a
regional scale, graben-bounding structure that separates Eocene
rocks to the west from Jurassic rocks to the east. Multiple zones
of silicification, clay alteration, brecciation and pyrite
mineralization, up to 42 m in core length, were intersected in
drilling. Although gold values were low, the trace element
signature to alteration in this area is identical to that of distal
alteration at the Main and 490 Zones. Significantly, the
geochemical signature here is several orders of magnitude greater
in strength than at the Main/490 Zones. Also significant is the
fact that this area is much higher in elevation than the Main/490
Zones. The distal geochemical signature of the alteration here
suggests a position too high in the epithermal system. The basal
controlling structure intersected in hole B14-11 to the alteration
did return 1.03 g/t Au over 0.5 m. A high priority for follow-up
drilling is to trace this controlling structure down-dip to the
west, to target a deeper level in the hydrothermal system.
Holes B14-07 and 14-12 were drilled 300-600 m north and
northwest of hole B14-06 and 500-900 m west of the Gossan Zone, to
test an IP chargeability anomaly in an area of structural interest.
Several zones of strong alteration, similar to that seen in other
holes, were encountered within permeable units. Hole B14-07 ended
at 326 m, with a 4 m interval grading 0.49 g/t Au. This zone
remains open to depth. Trace element geochemical vectoring from
these holes suggests a source located to the east, and may indicate
a common feeder structure to the alteration encountered to the east
in holes B14-08 through B14-11. A 500 m interval between holes
B14-11 and B14-12 remains untested by any drilling and is a high
priority target for follow-up.
All results exceeding a minimum of 0.25 g/t Au over a minimum 4
m interval are reported in the above table. High grade gold values
within these intervals are noted. Also reported are any samples
that returned greater than 1 g/t Au which are not part of larger
intervals meeting the cut-off threshold. Results for holes B14-01
through B14-05 have been previously released but are restated here
since follow-up analytical work may have resulted in minor
variations to originally reported intervals.
To view an enhanced version of Figure 2: Magnetic
Survey Map of Brett Gold Property, please visit:
http://orders.newsfilecorp.com/files/3028/14278_ximen.4.jpg
Intervals listed in this news release are core intervals. Grades
are weighted average grades over that interval. Further drilling is
required to determine the relationship between core interval and
true thickness. Sample intervals were determined by mineralization
and geology, but generally ranged from 0.5 to 2.0 meters. QA/QC
procedures were implemented in the drilling program, and included
company-inserted blanks and standards of known gold grade. Core was
sawn or split (depending on rock type), with half-core samples
delivered to ActLabs' Kamloops, B.C. laboratory (ISO 9001:2008
accredited, ISO 17025 pending) for preparation and analysis.
Generally, holes were sampled from top to bottom. In total, 1798
drill core samples, plus an additional 206 company inserted blanks
and standards, were submitted for analysis.
At the lab, samples were crushed to 90% passing a 2 mm screen,
then a 1 kg split of the crushed sample was pulverized to 95%
passing 105 microns. All samples were analysed for gold by FA/AA
finish on a 30 gram sample of pulverized material, and for a
multi-element suite by ICP-MS. Samples that returned > 2 ppm Au
by FA/AA were subsequently tested by metallic gold assay on a 500
gram sample of pulverized material. For samples reported in this
news release, gold values determined by metallic gold assay range
from -30% to +300% of gold values determined by FA/AA finish for
the same sample, with an average increase in gold grade of 63% by
the metallic gold assay method. Where metallic gold assays were
completed, those values have been used in the above quoted
intervals of average grade. Drilling was HQ sized core, reducing to
NQ2 where ground conditions dictated.
Linda Caron, M.Sc., P.Eng. is the Qualified Person under NI
43-101 who supervised the 2014 drill program and who has reviewed
and approved the technical content of this news release.
The Company further announces that it has amended and restated
its financial statements and management discussion and analysis for
the fiscal quarter ended September 30, 2015 to correct certain
accounting irregularities and has filed such statements under the
Company's profile on www.sedar.com.
About Ximen Mining Corp.
Ximen Mining Corp. owns 100 percent interest in its two
projects, Gold Drop Project and Brett Gold Project located in
southern British Columbia. Ximen is a publicly listed company
trading on the TSX Venture Exchange under the symbol XIM, and is
listed on the Frankfurt, Munich, and Berlin Stock Exchanges in
Germany under the symbol 1XM and WKN number is A1W2EG as well in
the USA under the symbol XXMMF.
On behalf of the Board of Directors, "Christopher R. Anderson"
Christopher R. Anderson, President, CEO and Director Ximen Mining
Corp.
This press release shall not constitute an offer to sell or the
solicitation of an offer to buy any securities, nor shall there be
any sale of securities in any state in the United States in which
such offer, solicitation or sale would be unlawful. The securities
referred to herein have not been and will not be registered under
the United States Securities Act of 1933, as amended, and may not
be offered or sold in the United States absent registration or an
applicable exemption from registration requirements.
Neither TSX Venture Exchange nor its Regulation Services
Provider (as that term is defined in the policies of the TSX
Venture Exchange) accepts responsibility for the adequacy or
accuracy of this release.
CONTACT: For further information contact:
Renmark Financial Communications Inc.
Barry Mire:
bmire@renmarkfinancial.com
Robert Thaemlitz:
rthaemlitz@renmarkfinancial.com
Tel.: (416) 644-2020 or (514) 939-3989
www.renmarkfinancial.com
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